| Literature DB >> 30910818 |
Masafumi Harada1,2, Kohei Ito1,2, Nobuyoshi Nakajima3, Shigeki Yamamura3,4, Masaru Tomita1,2, Haruo Suzuki5,2, Seigo Amachi6.
Abstract
Strain SCT is an iodate-reducing bacterium isolated from marine sediment in Kanagawa Prefecture, Japan. In this study, we determined the draft genome sequence of strain SCT and compared it to complete genome sequences of other closely related bacteria, including Pseudomonas stutzeri A phylogeny inferred from concatenation of core genes revealed that strain SCT was closely related to marine isolates of P. stutzeri Genes present in the SCT genome but absent from the other analyzed P. stutzeri genomes comprised clusters corresponding to putative prophage regions and possible operons. They included pil genes, which encode type IV pili for natural transformation; the mer operon, which encodes resistance systems for mercury; and the pst operon, which encodes a Pi-specific transport system for phosphate uptake. We found that strain SCT had more prophage-like genes than the other P. stutzeri strains and that the majority (70%) of them were SCT strain-specific. These genes, encoded on distinct prophage regions, may have been acquired after branching from a common ancestor following independent phage transfer events. Thus, the genome sequence of Pseudomonas sp. strain SCT can provide detailed insights into its metabolic potential and the evolution of genetic elements associated with its unique phenotype.Entities:
Keywords: Pseudomonas stutzeri; comparative genomics; gene conservation; genome analysis; iodate-reducing bacterium; marine sediment; phylogeny; strain SCT
Mesh:
Substances:
Year: 2019 PMID: 30910818 PMCID: PMC6505155 DOI: 10.1534/g3.118.200978
Source DB: PubMed Journal: G3 (Bethesda) ISSN: 2160-1836 Impact factor: 3.154
Genomic features of Pseudomonas strains analyzed
| Accession | Organism | Isolation source | Size (Mb) | ||||
|---|---|---|---|---|---|---|---|
| This study | Marine sediment | 4.79 | 62.5 | 4520 | 184 | 4520 | |
| GCF_000327065.1 | Cr(VI)-contaminated aquifer | 4.58 | 62.5 | 4353 | 43 | 3919 | |
| GCF_000661915.1 | Marine sediment | 4.73 | 62.3 | 4533 | 109 | 3678 | |
| GCF_000267545.1 | Marine sediment | 4.71 | 62.7 | 4417 | 95 | 3578 | |
| GCF_000195105.1 | Oil-contaminated soil | 4.65 | 64.0 | 4342 | 33 | 3547 | |
| GCF_001038645.1 | 4.69 | 64.0 | 4427 | 0 | 3560 | ||
| GCF_000219605.1 | Clinical specimen | 4.55 | 63.9 | 4242 | 23 | 3473 | |
| GCF_000013785.1 | Rice paddy soil | 4.57 | 63.9 | 4270 | 31 | 3461 | |
| GCF_000590475.1 | Soil | 4.73 | 60.6 | 4317 | 27 | 2367 | |
| GCF_001648195.1 | Marine sediment | 5.03 | 60.3 | 4687 | 77 | 2580 | |
| GCF_000279165.1 | Soil | 4.17 | 63.2 | 3931 | 0 | 2463 | |
| GCF_000818015.1 | Wastewater treatment plant | 4.38 | 64.0 | 4126 | 52 | 2522 | |
| GCF_000016565.1 | PCP-contaminated soil | 5.07 | 64.7 | 4714 | 68 | 1612 |
NCBI RefSeq accession number.
Percentage of G and C in the nucleotide sequence, defined as 100 × (G+C)/(A+T+G+C).
Number of protein-coding DNA sequences (CDSs).
Number of CDSs in phage-like regions predicted using PHASTER.
Number of SCT genes conserved in each genome inferred using LS-BSR.
Figure 1Maximum likelihood tree obtained from a concatenated nucleotide sequence alignment of core genes for the 13 Pseudomonas strains. The horizontal bar at the base of the figure represents 0.02 substitutions per nucleotide site. Bootstrap support values for each of the branches of the tree are indicated based on 100 bootstrap replicates. Blue represents strains isolated from water environments such as marine sediments.